Abstract:
:The well-known debate on the nature and origin of intracellular inclusions (ICIs) in silicified microfossils from the early Neoproterozoic Bitter Springs Formation has recently been revived by reports of possible fossilized nuclei in phosphatized animal embryo-like fossils from the Ediacaran Doushantuo Formation of South China. The revisitation of this discussion prompted a critical and comprehensive investigation of ICIs in some of the oldest indisputable eukaryote microfossils-the ornamented acritarchs Dictyosphaera delicata and Shuiyousphaeridium macroreticulatum from the Paleoproterozoic Ruyang Group of North China-using a suite of characterization approaches: scanning electron microscopy (SEM), transmission electron microscopy (TEM), and focused ion beam scanning electron microscopy (FIB-SEM). Although the Ruyang acritarchs must have had nuclei when alive, our data suggest that their ICIs represent neither fossilized nuclei nor taphonomically condensed cytoplasm. We instead propose that these ICIs likely represent biologically contracted and consolidated eukaryotic protoplasts (the combination of the nucleus, surrounding cytoplasm, and plasma membrane). As opposed to degradational contraction of prokaryotic cells within a mucoidal sheath-a model proposed to explain the Bitter Springs ICIs-our model implies that protoplast condensation in the Ruyang acritarchs was an in vivo biologically programmed response to adverse conditions in preparation for encystment. While the discovery of bona fide nuclei in Paleoproterozoic acritarchs would be a substantial landmark in our understanding of eukaryote evolution, the various processes (such as degradational and biological condensation of protoplasts) capable of producing nuclei-mimicking structures require that interpretation of ICIs as fossilized nuclei be based on comprehensive investigations.
journal_name
Geobiologyjournal_title
Geobiologyauthors
Pang K,Tang Q,Schiffbauer JD,Yao J,Yuan X,Wan B,Chen L,Ou Z,Xiao Sdoi
10.1111/gbi.12053subject
Has Abstractpub_date
2013-11-01 00:00:00pages
499-510issue
6eissn
1472-4677issn
1472-4669journal_volume
11pub_type
杂志文章相关文献
Geobiology文献大全abstract::Ediacaran sediments record an unusual global carbon cycle perturbation that has been linked to widespread oceanic oxygenation, the Shuram negative C isotope excursion (NCIE). However, proxy-based estimates of global ocean redox conditions during this event have been limited largely due to proxy specificity (e.g., euxi...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12379
更新日期:2020-05-01 00:00:00
abstract::A combination of scanning transmission X-ray microscopy and X-ray magnetic circular dichroism was used to spatially resolve the distribution of different carbon and iron species associated with Shewanella oneidensis MR-1 cells. S. oneidensis MR-1 couples the reduction of Fe(III)-oxyhydroxides to the oxidation of organ...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/j.1472-4669.2012.00329.x
更新日期:2012-07-01 00:00:00
abstract::The Atacama Desert is the driest non-polar desert on Earth, presenting precarious conditions for biological activity. In the arid coastal belt, life is restricted to areas with fog events that cause almost daily wet-dry cycles. In such an area, we discovered a hitherto unknown and unique ground covering biocenosis dom...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12368
更新日期:2020-01-01 00:00:00
abstract::Microbial fossils and textures are commonly preserved in Ediacaran and early Cambrian coarse-grained siliciclastic sediments that were deposited in tidal and intertidal marine settings. In contrast, the fossilization of micro-organisms in similar marine environments of post-Cambrian age is less frequently reported. Th...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12229
更新日期:2017-07-01 00:00:00
abstract::The Strelley Pool Formation (SPF) is widely distributed in the East Pilbara Terrane (EPT) of the Pilbara Craton, Western Australia, and represents a Paleoarchean shallow-water to subaerial environment. It was deposited ~3.4 billion years ago and displays well-documented carbonate stromatolites. Diverse putative microf...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12148
更新日期:2015-11-01 00:00:00
abstract::Biogeochemical changes in marine sediments during coastal water hypoxia are well described, but less is known about underlying changes in microbial communities. Bacterial and archaeal communities in Louisiana continental shelf (LCS) hypoxic zone sediments were characterized by pyrosequencing 16S rRNA V4-region gene fr...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12142
更新日期:2015-09-01 00:00:00
abstract::The period 800-717 million years (Ma) ago, in the lead-up to the Sturtian Snowball glaciation, saw an increase in the diversity of eukaryotic microfossils. To afford an independent and complementary view of this evolutionary period, this study presents the distribution of eukaryotic biomarkers from three pre-Sturtian ...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12165
更新日期:2016-03-01 00:00:00
abstract::The diagenetic mineral assemblages in petroleum reservoirs control the formation fluid pH and pCO(2). Anaerobic biodegradation of petroleum is controlled by the transfer of electrons from reduced organic species to inorganic, redox sensitive, aqueous and mineral species in many cases through intermediates such as H(2)...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/j.1472-4669.2009.00224.x
更新日期:2010-01-01 00:00:00
abstract::Meromictic lakes with anoxic bottom waters often have active methane cycles whereby methane is generally produced biogenically under anoxic conditions and oxidized in oxic surface waters prior to reaching the atmosphere. Lakes that contain dissolved ferrous iron in their deep waters (i.e., ferruginous) are rare, but v...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12365
更新日期:2020-01-01 00:00:00
abstract::Ocean acidification by atmospheric carbon dioxide has increased almost continuously since the last glacial maximum (LGM), 21,000 years ago. It is expected to impair tropical reef development, but effects on reefs at the present day and in the recent past have proved difficult to evaluate. We present evidence that acid...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12097
更新日期:2014-09-01 00:00:00
abstract::The persistence of DNA from microorganisms exposed to various concentrations of SiO2 (ranging from 0 to 3000 p.p.m.) was monitored over time. The impact of silica mineralization or silicification on the longevity of 16S rRNA and 16 s rDNA genes from whole cells of Bacillus subtilis and Escherichia coli K12 was quantif...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/j.1472-4669.2008.00177.x
更新日期:2008-12-01 00:00:00
abstract::We established Fe(III)-reducing co-cultures of two species of metal-reducing bacteria, the Gram-positive Desulfotomaculum reducens MI-1 and the Gram-negative Geobacter sulfurreducens PCA. Co-cultures were given pyruvate, a substrate that D. reducens can ferment and use as electron donor for Fe(III) reduction. G. sulfu...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12295
更新日期:2018-09-01 00:00:00
abstract::Mixing of sediments by moving animals becomes apparent in the trace fossil record from about 550 million years ago (Ma), loosely overlapping with the tail end of the extreme carbonate carbon isotope δ13 Ccarbonate fluctuations that qualitatively distinguish the Proterozoic geochemical record from that of the Phanerozo...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12277
更新日期:2018-05-01 00:00:00
abstract::We here show that nano-scale mapping of elements commonly utilized in biological cycles provides a promising new additional line of evidence when evaluating the extent of the contribution of biology to microbialites. Our case study comes from Lake Clifton in Western Australia, a unique environment where living domical...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/j.1472-4669.2010.00251.x
更新日期:2010-12-01 00:00:00
abstract::Evaporitic deposits are a globally widespread habitat for micro-organisms. The microbe-mineral environment in weathered and remobilized gypsum from exposed mid-Ordovician marine evaporite beds in the polar desert of Devon Island, Nunavut, Canadian High Arctic was examined. The gypsum is characterized by internal green...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/j.1472-4669.2010.00240.x
更新日期:2010-09-01 00:00:00
abstract::The later Cambrian Steptoean Positive Carbon Isotope Excursion (SPICE) event was an episode marked by pronounced changes to the global biogeochemical cycles of carbon and sulfur and significant extinctions on several paleocontinents including Laurentia (North America). While the exact cause(s) of these events remains ...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12334
更新日期:2019-07-01 00:00:00
abstract::The ca. 1.9 Ga Beaverlodge Lake paleosol was studied using redox-sensitive Cr isotopes in order to determine the isotopic response to paleoweathering of a rhyodacite parent rock 500 million years after the Great Oxidation Event. Redox reactions occurring in modern weathering environments produce Cr(VI) that is enriche...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12342
更新日期:2019-09-01 00:00:00
abstract::Subseafloor sulfate concentrations typically decrease with depth as this electron acceptor is consumed by respiring microorganisms. However, studies show that seawater can flow through hydraulically conductive basalt to deliver sulfate upwards into deeply buried overlying sediments. Our previous work on IODP Site C001...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12324
更新日期:2019-03-01 00:00:00
abstract::In the aftermath of the end-Permian mass extinction, Early Triassic sediments record some of the largest Phanerozoic carbon isotopic excursions. Among them, a global Smithian-negative carbonate carbon isotope excursion has been identified, followed by an abrupt increase across the Smithian-Spathian boundary (SSB; ~250...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12174
更新日期:2016-05-01 00:00:00
abstract::Ooids from the Mesoarchaean Chobeni Formation, Pongola Supergroup, KwaZulu-Natal, South Africa are older than any ooids reported to date. They are made of dolomite and ankerite and show concentric, radial-concentric, micritic, and radial fabrics. Radial ooids are interpreted to have originated from high-Mg-calcite and...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12249
更新日期:2017-11-01 00:00:00
abstract::Although nitrogen is a key element in organic molecules such as nucleic acids and proteins, the timing of the emergence of its modern biogeochemical cycle is poorly known. Recent studies on the antiquity of the nitrogen cycle and its interaction with free oxygen suggests the establishment of a complete aerobic N bioge...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/j.1472-4669.2011.00271.x
更新日期:2011-03-01 00:00:00
abstract::Previous studies of the subsurface biosphere have deduced average cellular doubling times of hundreds to thousands of years based upon geochemical models. We have directly constrained the in situ average cellular protein turnover or doubling times for metabolically active micro-organisms based on cellular amino acid a...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12069
更新日期:2014-01-01 00:00:00
abstract::All life requires energy to drive metabolic reactions such as growth and cell maintenance; therefore, fluctuations in energy availability can alter microbial activity. There is a gap in our knowledge concerning how energy availability affects the growth of extreme chemolithoautotrophs. Toward this end, we investigated...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12413
更新日期:2021-01-01 00:00:00
abstract::The paleoenvironmental setting in which the Ediacara Biota lived, died, and was preserved in the eponymous Ediacara Member of the Rawnsley Quartzite of South Australia is an issue of long-standing interest and recent debate. Over the past few decades, interpretations have ranged from deep marine to shallow marine to t...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12262
更新日期:2018-01-01 00:00:00
abstract::The dissolution of elemental selenium [Se(0)] during chemical weathering is an important step in the global selenium cycle. While microorganisms have been shown to play a key role in selenium dissolution in soils, the mechanisms of microbial selenium solubilization are poorly understood. In this study, we isolated a B...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12328
更新日期:2019-05-01 00:00:00
abstract::The composition of the oceans and of its biota have influenced each other through Earth's history. Of all the biologically essential elements, nitrogen is the only one whose seawater concentration is clearly controlled biologically; this is presumably the main reason why the stoichiometry of nitrogen (defined as its m...
journal_title:Geobiology
pub_type: 杂志文章,评审
doi:10.1111/j.1472-4669.2008.00144.x
更新日期:2008-06-01 00:00:00
abstract::Microfossils belonging to the 1.88-billion-year-old 'Gunflint-biota' are preserved as carbonaceous and hematitic filaments and spheres that are believed to represent ancient chemolithoautotrophic Fe(II) oxidizing bacteria that grew above a chemocline where ferruginous seawater upwelled into shallow, oxygenated waters....
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12127
更新日期:2015-05-01 00:00:00
abstract::Few topics in geobiology have been as extensively debated as the role of Earth's oxygenation in controlling when and why animals emerged and diversified. All currently described animals require oxygen for at least a portion of their life cycle. Therefore, the transition to an oxygenated planet was a prerequisite for t...
journal_title:Geobiology
pub_type: 杂志文章,评审
doi:10.1111/gbi.12382
更新日期:2020-05-01 00:00:00
abstract::New experimental results of fluid-mineral reactions at hydrothermal conditions relevant to life demonstrate that key redox reactions involving iron, sulfur, and hydrogen remain at disequilibrium at 100 °C, even in a heterogeneous system and thus are energetically favorable for microbial metabolism. Predictions from ge...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/j.1472-4669.2010.00255.x
更新日期:2010-12-01 00:00:00
abstract::The hydrocarbons preserved in an Archean rock were extracted, and their composition and distribution in consecutive slices from the outside to the inside of the rock were examined. The 2.7 Ga rock was collected from the Fortescue Group in the Pilbara region, Western Australia. The bitumen I (solvent-extracted rock) an...
journal_title:Geobiology
pub_type: 杂志文章
doi:10.1111/gbi.12117
更新日期:2015-03-01 00:00:00